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Abstract:

The magmatic arc of the Fuegian Andes is composed mostly of Upper Mesozoic to Cenozoic calc-alkaline plutons and subordinated lavas. To the rear arc, however, isolated mid-Cretaceous monzonitic plutons and small calc-alkaline dykes and sills crop out. This calc-alkaline unit (the Ushuaia Peninsula Andesites, UPA) includes hornblende-rich, porphyritic quartz meladiorites, granodiorites, andesites, dacites and lamprophyres. Radiometric dating and cross-cutting relationships indicate that UPA is younger than the monzonitic suite. The geochemistry of UPA is medium to high K, with high LILE (Ba 500-2000 ppm, Sr 800-1400 ppm), HFSE (Th 7-23 ppm, Nb 7-13 ppm, Ta 0.5-1.1 ppm) and LREE (La 16-51 ppm) contents, along with relatively low HREE (Yb 1.7-1.3 ppm) and Y (9-19 ppm). The similar mineralogy and geochemistry of all UPA rocks suggest they evolved from a common parental magma, by low pressure crystal fractionation, without significant crustal assimilation. A pure Rayleigh fractionation model indicates that 60-65% of crystal fractionation of 60% hornblende + 34% plagioclase + 4% clinopyroxene + 1% Fe-Ti oxide, apatite and sphene (a paragenesis similar of UPA mafic rocks) can explain evolution from lamprophyres to dacites. The UPA has higher LILE, HFSE and LREE, and lower HREE and Y than the calc-alkaline plutons and lavas of the volcanic front. The HREE and Y are lower than in the potassic plutons as well. High concentrations of Th, Nb, Ta, Zr, Hf, LREE and Ce/Pb, and low U/Th, Ba/Th ratios in UPA, even in the least differentiated samples, suggest contributions from subducted sediments to the mantle source. On the other hand, relatively low HREE and Y, high LREE/HREE (La/Yb 11-38) ratios and Nb-Ta contents can be interpreted as mantle metasomatism by partial melts of either subducted garnetiferous oceanic sediment or basalt as well. Additionally, high LILE content in UPA, similar to the potassic plutons, suggests also a mantle wedge previously metasomatized by potassic parental magmas in their route to crustal levels. Therefore, UPA represents a unique suite in the Fuegian arc generated in a multiple hybridized source. UPA generation is related to a transition from normal to flat subduction which additionally caused the widening and landward migration of the magmatic arc, as well as crustal deformation. Rear-arc magmatism endured ca. 22 m.y.; afterwards, calc-alkaline magmatism remained at the volcanic front. © 2010 Elsevier Ltd.

Registro:

Documento: Artículo
Título:Calc-alkaline rear-arc magmatism in the Fuegian Andes: Implications for the mid-cretaceous tectonomagmatic evolution of southernmost South America
Autor:Guillot, M.G.; Escayola, M.; Acevedo, R.
Filiación:Centro Austral de Investigaciones Científicas (CADIC), CONICET, B. Houssay 200, (V9410BFD) Ushuaia, Argentina
Laboratorio de Tectónica Andina, Universidad de Buenos Aires, Ciudad Universitaria Pabellón II, C1428EHA, Argentina
Palabras clave:Fuegian Andes; Rear-arc magmatism; Slab flattening; Source enrichment; calc alkaline rock; Cretaceous; crustal deformation; geochemistry; geochronology; magmatism; mineralogy; pluton; subduction; tectonic evolution; Andes
Año:2011
Volumen:31
Número:1
Página de inicio:1
Página de fin:16
DOI: http://dx.doi.org/10.1016/j.jsames.2010.11.002
Título revista:Journal of South American Earth Sciences
Título revista abreviado:J. South Am. Earth Sci.
ISSN:08959811
Registro:https://bibliotecadigital.exactas.uba.ar/collection/paper/document/paper_08959811_v31_n1_p1_Guillot

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Citas:

---------- APA ----------
Guillot, M.G., Escayola, M. & Acevedo, R. (2011) . Calc-alkaline rear-arc magmatism in the Fuegian Andes: Implications for the mid-cretaceous tectonomagmatic evolution of southernmost South America. Journal of South American Earth Sciences, 31(1), 1-16.
http://dx.doi.org/10.1016/j.jsames.2010.11.002
---------- CHICAGO ----------
Guillot, M.G., Escayola, M., Acevedo, R. "Calc-alkaline rear-arc magmatism in the Fuegian Andes: Implications for the mid-cretaceous tectonomagmatic evolution of southernmost South America" . Journal of South American Earth Sciences 31, no. 1 (2011) : 1-16.
http://dx.doi.org/10.1016/j.jsames.2010.11.002
---------- MLA ----------
Guillot, M.G., Escayola, M., Acevedo, R. "Calc-alkaline rear-arc magmatism in the Fuegian Andes: Implications for the mid-cretaceous tectonomagmatic evolution of southernmost South America" . Journal of South American Earth Sciences, vol. 31, no. 1, 2011, pp. 1-16.
http://dx.doi.org/10.1016/j.jsames.2010.11.002
---------- VANCOUVER ----------
Guillot, M.G., Escayola, M., Acevedo, R. Calc-alkaline rear-arc magmatism in the Fuegian Andes: Implications for the mid-cretaceous tectonomagmatic evolution of southernmost South America. J. South Am. Earth Sci. 2011;31(1):1-16.
http://dx.doi.org/10.1016/j.jsames.2010.11.002